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Subaqueous Delta of the Ganges-Brahmaputra River System

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Subaqueous Delta of the Ganges-Brahmaputra River System ELSEVIER Marine Geology 144 (1997) 81-96 Subaqueous delta of the Ganges-Brahmaputra river system Steven A. Kuehl a,*, Beth M. Levy a, Willard S. Moore b, Mead A. Allison ’ a Virginia Institute of Marine Science, College of William and Mary, Gloucester Point, VA 23062, USA b Department of Geological Sciences, University of South Carolina, Columbia, SC29208, USA ’ Department of Oceanography, Texas A&M University, 5007 Avenue U. Galveston, TX 77551. USA Received 19 July 1996; accepted 16 June 1997 Abstract The Ganges-Brahmaputra is among the world’s three largest river systems in terms of sediment load, but, until now, no high-resolution seismic data have been obtained to document the nature of the sediment deposit seaward of the rivers’ mouths. The other two (Amazon, Huanghe) discharge into energetic coastal environments and form subaqueous deltas with characteristic clinoform stratigraphy. High-resolution seismic reflection profiles of the Bengal shelf reveal similar stratigraphy: topset beds dip gently (0.036”) and diverge offshore; more steeply dipping foreset beds (0.190”) converge farther seaward; and relatively thin, gently dipping bottomset beds (0.022”) extend across the outer shelf, overlying an erosional surface presumed to be of Late Pleistocene age. Sediment accumulation rates are highest in the foreset region (2 5 cm/year) and reduced in the bottomset region (co.3 cm/year), corroborating the relative thickening and thinning of strata observed in seismic profiles. Taken together, these data indicate a subaqueous delta is actively prograding across the Bengal shelf. Volume estimates for the Holocene subaqueous delta reveal that about one third of the total load of the Ganges-Brahmaputra has accumulated on the shelf. The remainder is likely partitioned between the river floodplain/delta plain and off-shelf transport via the submarine canyon, Swatch of No Ground. The canyon incises the shelf in the area of highest sedimentation rates (foreset), and growth faults and slumping of modern sediments near the head of the canyon support the idea that significant off-shelf transport of sediments to the Bengal Fan is occurring. 0 1997 Elsevier Science B.V. Keywords: delta; shelf sedimentation; seismic reflection profiling; sediment budget; Bay of Bengal; Ganges River; Brahmaputra River 1. Introduction delta, commonly are found in quiescent seas or protected locations such as fjords and embay- Modern river deltas have a range of characteris- ments. Rivers entering energetic marine environ- tic morphologies that, to a first approximation, ments display a variety of morphologies. For are controlled by the fluvial, tidal, and wave regime example, the Columbia River (Northwest coast, (Wright and Coleman, 1973). Deltas with extens- U.S.A.) has no subaerial delta, rather, accumula- ive subaerial expression, such as the Mississippi tion occurs as a mid-shelf mud deposit (Wright and Nittrouer, 1995). Rivers with sediment loads * Corresponding author. Fax: + 1 (804) 684 7250: comparable to the Ganges-Brahmaputra, such as e-mail: [email protected] the Amazon and Huanghe, exhibit predominant 0025-3227/97/$17.00 0 1997 Elsevier Science B.V. All rights reserved PII SOO25-3227(97)00075-3 or partial subaqueous growth of their deltas, seaward of the Ganges-Brahmaputra river system. respectively (Nittrouer et al., 1986; Prior et al.. In addition, sediment cores collected from the shelf 1986; Alexander et al., 1991 ). Even though the are used to examine the distribution of recent sediment discharge of the Amazon is sufficient to accumulation rates in relation to seismic observa- produce a sizable subaqueous delta (clinoform) on tions. The objectives are to examine the idea that the shelf, large shear stresses, generated primarily a major component of the Ganges-Brahmaputra by tides, appear to prevent or limit significant delta occurs on the shelf as a subaqueous clinoform subaerial growth in the vicinity of the river’s mouth and to evaluate the role of the Swatch of No (Kuehl et al., 1986; Geyer et al., 1996). For the Ground as a potential conduit for bypassing Huanghe, about lo--15% of the sediment discharge modern river sediments to the Bengal Fan. accumulates south of the Shangdong Peninsula as a subaqueous delta (Alexander et al., 1991), with much of the remaining discharge contributing to 2. Background rapid subaerial growth. This dual-mode prograda- tion of the delta reflects the phasing of river .?. 1. River churucteristics urd Holocvnr discharge and energy conditions in the Gulf of .strutigrctph~~qf thu delta Bohai; high discharge occurs during low-energy conditions resulting in deposition near the mouth The Ganges, Brahmaputra and Meghna rivers and significant subaerial growth (Wright and have occupied and abandoned numerous courses Nittrouer, 1995 ). during the Quaternary and have deposited a large. Although the combined sediment discharge of flat, low-lying alluvial/delta plain encompassing the Ganges-Brahmaputra river system is among most of the country of Bangladesh (Coleman, the world’s largest and its delta plain among the 1969). The Ganges drains the south slopes of the world’s most densely populated, little is known Himalayan mountains whereas the Brahmaputra regarding the Holocene evolution of the delta or mostly drains the north slopes, with estimated the processes and patterns of recent deltaic sedi- suspended sediment loads of 520 x lo6 t/year and mentation. Based on examination of nautical 540 x lo6 t/year, respectively (Milliman and charts dating back some 200 years, Coleman Syvitski, 1992). The Meghna River drains north- ( 1969) suggested that no significant seaward pro- eastern Bangladesh but has a negligible impact on gradation of the shoreline had occurred and that the combined load of the system, contributing sediments discharged to the coastal ocean therefore only about 1% of the total sediment discharge escaped to the deep sea through the Swatch of No (Coleman, 1969). Combined monthly sediment Ground, a major submarine canyon feeding the and water discharge reaches a maximum in August immense Bengal Fan. A recent critical examination during the southwest monsoon, with minimal levels of a more extensive set of historical charts. how- (an order of magnitude less than peak rates) in ever, has provided evidence for some recent growth January-March. Suspended sediments of the of the subaerial delta, but with progradation occur- Ganges-Brahmaputra are coarse relative to other ring in a lateral (west to east) fashion (Allison. large river systems; at the confluence of the Ganges 1997). Preliminary study of the continental shelf and Brahmaputra about 40% is sand (mostly seaward of the rivers’ mouths revealed significant fine-very fine) and 60% silt-clay (Barua et al.. sediment accumulation, leading to the suggestion 1998). that the observed clinoform-like morphology Umitsu ( 1985, 1987, 1993) divided the land- reflects the presence of an active subaqueous delta forms of the Bengal Basin into two geomorphologi- (Kuehl et al., 1989). However, until now, no cal units: Pleistocene terrace uplands and recent seismic data have been obtained to document the alluvial lowlands (Fig. 1). The Pleistocene terraces stratigraphic nature of this feature. Here we report are found in the marginal and interior portions of the results of the first high-resolution seismic the Basin. In the north the uplands are known as reflection study conducted on the Bengal shelf the Barind Tract. and as the Madhupur Terrace S. A. Kuehl et al. / Marine Geology 144 (19971 81-96 83 WE 89” 90” 91" 92” 26”N 26”N 25’ ‘25” 24O 24” 23” 23’ 22” 21” 8&E QiY Fig. 1. Physiographic map of the Ganges-Brahmaputra delta. in the central region. Alluvial lowlands are distrib- last glacial maximum (Umitsu, 1993). The lowest uted widely over the Bengal Basin with characteris- unit dates from the last glacial maximum and tic levees, point bars and channel bars, as well as consists of sandy gravels deposited by the rivers lower landform units such as swamps, marshes down cutting older surfaces. Radiocarbon dating and former river channels. Sediments consist and similarities in sediment facies and grain size mainly of sand, silt, and clay layers with peat of the lower unit near Khulna City with that of layers recognized in several places. The elevation the present Brahmaputra River flood plain suggest of the lowlands typically is < 15 m above sea level that this unit represents the flood plain about and most of the southern region is < 3 m above 12,000 years before present. The middle unit is sea level. composed of fine deltaic sediments deposited Five stratigraphic units characterize the evolu- during the transgression. Peat layers are found in tion of the Ganges-Brahmaputra delta since the the Sylhet Basin in the lower horizon of the unit, indicating the presence of marshes during this western region. Spring winds. combined with the period. The lower portion of the upper unit (mid- Coriolis effect, result in the movement of surface Holocene) is comprised of silt and clay in the water away from the east Indian coast with deeper inland region of Tangail; however, near the more water upwelling, causing the isopycnals to tilt coastal region of Khulna, the sediments exhibit a upward towards the Indian coast. In the autumn. strong marine influence. Umitsu ( 1993) proposed the reverse occurs as water is piled up in the that the coastline at that time retreated slightly western part of the bay and the isopycnals tilt north of the present Khulna City. The upper down toward the east Indian coast. Resulting portions of the upper unit become coarser. with seasonal changes in sea level exceed 1 m for the peat in places, suggesting that the coastline pro- northeast coast at Chittagong and along southeast graded during this time as broad marshy peat Bangladesh, the largest on record (Murty et al.. lands covered the central Ganges-Brahmaputra 1992). Observations and modeling of the fresh delta.
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